muschelkalk การใช้
- Especially susceptible are steep rock faces in Muschelkalk and White Jurassic.
- Ridges of Muschelkalk limestone are found mainly in the Thuringian Basin.
- The muschelkalk-new red sandstone mineral boundary was crossed.
- Formerly the middle series in the Triassic was also known as Muschelkalk.
- The region forms part of the larger Muschelkalk geological zone.
- The Muschelkalk in the other tunnel also required special care.
- The gau landscape is mainly characterised by heavy muschelkalk soils.
- The basin in which the Muschelkalk was deposited is called the Germanic Basin.
- Species of orchid abound on the open Muschelkalk slopes.
- The Erfurt Formation is underlain by the Upper Muschelkalk.
- The lithostratigraphic status of the Muschelkalk differs regionally.
- Farther east in the Bauland, the muschelkalk deposits still overlie the Early Triassic layers.
- The " kuppen " and plateaux rest directly on a bedrock of muschelkalk.
- Later, during the Zechstein and Muschelkalk the region was largely flooded by the sea.
- It is chiefly composed of bunter sandstone and muschelkalk and has been designated a protected area.
- The basement is formed of red clays and marls overlaid by rocks of the Lower Muschelkalk.
- Again the keuper escarpment is missing and even the muschelkalk only appears in islands around individual domes.
- In the Middle Muschelkalk, weathering can form characteristic cellular dolostone ( " Zellendolomit " ).
- Within the North French Scarplands it represents the Muschelkalk stage, but also transitions locally into bunter sandstone.
- On the muschelkalk lands of today s Bauland, which favoured agriculture, a broad mesh of settlements arose.
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